Geology of Serbia

Mountain ranges of Serbia

The regional geology of Serbia describes the geologic structure and history inside the borders of Serbia.

Serbia is in recent geologic time a part of the Eurasian Plate, but the bedrock lithologies are witness to a diverse geologic history.[1] In a tectonic sense, Serbia is part of an orogenic system that is composed of the Alpine, Carpathian, and Dinaride orogenic belts.[2][3] Its territory can be divided into five geotectonic units of differing genesis:[4][5]

  1. ^ "Tectonic Plates: Divergent, Convergent, and Transform Boundaries" (PDF) (Map). Tectonics Observatory. California Institute of Technology. April 2009. Retrieved 19 September 2013.
  2. ^ Schmid, Stefan M.; Daniel Bernoulli; Bernhard Fügenschuh; Liviu Matenco; Senecio Schefer; Ralf Schuster; Matthias Tischler; Kamil Ustaszewski (2008). "The Alpine-Carpathian-Dinaridic orogenic system: correlation and evolution of tectonic units" (PDF). Swiss Journal of Geosciences. 101 (1): 139–183. doi:10.1007/s00015-008-1247-3. S2CID 55108896.
  3. ^ Milena Zlokolica-Mandic. "Structural-Tectonic Elements as a Factor in Cave Development". Serbian Academy of Sciences and Arts. Archived from the original on 27 July 2011. Retrieved 3 November 2010.
  4. ^ Mica Martinovic; Mihailo Milivojevic (25 April 2010). "Serbia Country Update" (PDF). Proceedings of World Geothermal Congress 2010. Archived from the original (PDF) on 22 July 2011.
  5. ^ Eldridge M. Moores; Rhodes Whitmore Fairbridge (1997). Encyclopedia of European and Asian regional geology. Springer. pp. 786–789. ISBN 978-0-412-74040-4.

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